Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
QUICK SEARCH:   [advanced]


     

Bulletin of the Seismological Society of America; February 1973; v. 63; no. 1; p. 101-104
© 1973 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by MOLNAR, P.
Right arrow Articles by MCCAMY, K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Implications of Archambeau's earthquake source theory for slip on faults

PETER MOLNAR, KLAUS H. JACOB and KEITH MCCAMY

INSTITUTE OF GEOPHYSICS AND PLANETARY PHYSICS UNIVERSITY OF CALIFORNIA, SAN DIEGO, LA JOLLA, CALIFORNIA 92037
LAMONT-DOHERTY GEOLOGICAL OBSERVATORY OF COLUMBIA UNIVERSITY, PALISADES, NEW YORK 10964

Abstract

Archambeau's source theory predicts a distinct peak in the displacement amplitude spectrum of body waves radiated into the far-field. If the assumption that earthquakes may alternatively be described by dislocation theory is valid, then this peak in the spectrum can occur only (1) if different parts of the fault, but on the same side of the fault, slip in opposite directions or (2) if the fault slips back after exceeding the maximum displacement. Data at the present time do not provide strong evidence for a peak in the displacement spectrum. The peak in Archambeau's spectrum may be caused by the absence of frictional damping in his model.




This article has been cited by other articles:


Home page
 Bulletin of the Seismological Society of AmericaHome page
K. AKI
Source and scatering effects on the spectra of small local earthquakes
Bulletin of the Seismological Society of America, December 1, 1981; 71(6): 1687 - 1700.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
B. CHOUET, K. AKI, and M. TSUJIURA
Regional variation of the scaling law of earthquake source spectra
Bulletin of the Seismological Society of America, February 1, 1978; 68(1): 49 - 79.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
T. C. BACHE
The effect of tectonic stress release on explosion P-wave signatures
Bulletin of the Seismological Society of America, October 1, 1976; 66(5): 1441 - 1457.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
D. J. ANDREWS
From antimoment to moment: Plane-strain models of earthquakes that stop
Bulletin of the Seismological Society of America, February 1, 1975; 65(1): 163 - 182.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
F. A. DAHLEN
On the ratio of P-wave to S-wave corner frequencies for shallow earthquake sources
Bulletin of the Seismological Society of America, August 1, 1974; 64(4): 1159 - 1180.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
D. M. BOORE and M. D. ZOBACK
Near-field motions from kinematic models of propagating faults
Bulletin of the Seismological Society of America, April 1, 1974; 64(2): 321 - 342.
[Abstract] [PDF]


HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1973 by the Seismological Society of America.